Abstract
Climatologies of aerosol backscatter profiles, derived from airborne and ground-based CO2 lidar returns, indicate a high frequency of occurrence for a narrow range of low backscatter values within the troposphere—a background mode.
© 1989 Optical Society of America
Full Article | PDF ArticleMore Like This
Vandana Srivastava, Maurice A. Jarzembski, and David A. Bowdle
Appl. Opt. 31(12) 1904-1906 (1992)
Robert T. Menzies and David M. Tratt
Appl. Opt. 33(24) 5698-5711 (1994)
John L. Gras and William D. Jones
Appl. Opt. 28(5) 852-856 (1989)